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• W659235061 startingPage "109" @default.
• W659235061 abstract "The Red Sea displays lithosphere that is in transition from rifting to drifting and therefore provides enormous opportunity to understand incipient seafloor spreading development. Despite more than 50 years of extensive geological and geophysical research, there remains significant conjecture concerning the timing of sea-floor spreading initiation, the extent of spreading along the axis of the Red Sea, and the geodynamic processes responsible for the onset of crustal extension. Red Sea tectonic models based on geological data are dominated by single stage rift models involving protracted stretching of continental crust followed by sea floor spreading at ca 5 Ma, and include both asymmetric and symmetrical extension models. Geophysical data suggest that an oceanic crust occurs beneath the Red Sea shelves, although exactly how this crust has evolved remains undecided. Equally, arguments have been made in favor of the sedimentary shelves forming on extended continental crust, and that oceanic crust is restricted to the present day Red Sea axial valley. However, our synthesis shows that none of the models proposed so far is applicable to the entire Red Sea basin. The distribution and timing of the Red Sea crustal extension and sea-floor spreading may have been influenced by subduction-related far field forces due to complex plate interactions along the northern edge of the Arabian plate during Early Miocene. Our reassessment suggests that following the arrival of the Afar plume the southern Red Sea underwent rapid extension culminating in the transition from rifting to seafloor spreading, which stalled during the early Miocene in the central Red Sea due to either slowing of the convergence between Arabia and Eurasia or the onset of the Arabian plate passive margin collision with Eurasia. Off axis magmatism is focused on the Arabian margin and Afar depression and has been episodically active since the Miocene. We consider a formation of the Red Sea as a hybrid process involving both “active and passive” rifting." @default.
• W659235061 created "2016-06-24" @default.
• W659235061 creator A5001847183 @default.
• W659235061 creator A5035161425 @default.
• W659235061 creator A5074885968 @default.
• W659235061 date "2015-08-01" @default.
• W659235061 modified "2023-10-18" @default.
• W659235061 title "The Red Sea – 50 years of geological and geophysical research" @default.
• W659235061 cites W1519872695 @default.
• W659235061 cites W1576516474 @default.
• W659235061 cites W1577670450 @default.
• W659235061 cites W1583837434 @default.
• W659235061 cites W1586341875 @default.
• W659235061 cites W1587864144 @default.
• W659235061 cites W1965374961 @default.
• W659235061 cites W1967824544 @default.
• W659235061 cites W1968534064 @default.
• W659235061 cites W1971284143 @default.
• W659235061 cites W1972081641 @default.
• W659235061 cites W1973778260 @default.
• W659235061 cites W1975351330 @default.
• W659235061 cites W1976823169 @default.
• W659235061 cites W1978317429 @default.
• W659235061 cites W1978632315 @default.
• W659235061 cites W1978905410 @default.
• W659235061 cites W1979407478 @default.
• W659235061 cites W1981175130 @default.
• W659235061 cites W1981675402 @default.
• W659235061 cites W1983393426 @default.
• W659235061 cites W1983510433 @default.
• W659235061 cites W1985368150 @default.
• W659235061 cites W1988125747 @default.
• W659235061 cites W1988780968 @default.
• W659235061 cites W1990442300 @default.
• W659235061 cites W1991520948 @default.
• W659235061 cites W1991924753 @default.
• W659235061 cites W1992272017 @default.
• W659235061 cites W1992477749 @default.
• W659235061 cites W1993524516 @default.
• W659235061 cites W1995172982 @default.
• W659235061 cites W1998184832 @default.
• W659235061 cites W1998759441 @default.
• W659235061 cites W2000339958 @default.
• W659235061 cites W2000984331 @default.
• W659235061 cites W2001636832 @default.
• W659235061 cites W2003987543 @default.
• W659235061 cites W2004717728 @default.
• W659235061 cites W2006254584 @default.
• W659235061 cites W2007143544 @default.
• W659235061 cites W2008069601 @default.
• W659235061 cites W2012530126 @default.
• W659235061 cites W2012770129 @default.
• W659235061 cites W2014552552 @default.
• W659235061 cites W2017695437 @default.
• W659235061 cites W2018383784 @default.
• W659235061 cites W2022061975 @default.
• W659235061 cites W2022648729 @default.
• W659235061 cites W2027226653 @default.
• W659235061 cites W2027477351 @default.
• W659235061 cites W2028324772 @default.
• W659235061 cites W2029779542 @default.
• W659235061 cites W2030629162 @default.
• W659235061 cites W2031815022 @default.
• W659235061 cites W2033507848 @default.
• W659235061 cites W2035284349 @default.
• W659235061 cites W2035525174 @default.
• W659235061 cites W2038342550 @default.
• W659235061 cites W2038658947 @default.
• W659235061 cites W2040123418 @default.
• W659235061 cites W2042055852 @default.
• W659235061 cites W2046640225 @default.
• W659235061 cites W2051046669 @default.
• W659235061 cites W2051870429 @default.
• W659235061 cites W2053090819 @default.
• W659235061 cites W2053596635 @default.
• W659235061 cites W2057186874 @default.
• W659235061 cites W2058884294 @default.
• W659235061 cites W2060405276 @default.
• W659235061 cites W2061754414 @default.
• W659235061 cites W2064119724 @default.
• W659235061 cites W2064307491 @default.
• W659235061 cites W2064401694 @default.
• W659235061 cites W2065992862 @default.
• W659235061 cites W2069684629 @default.
• W659235061 cites W2069875122 @default.
• W659235061 cites W2070249218 @default.
• W659235061 cites W2073470939 @default.
• W659235061 cites W2074029267 @default.
• W659235061 cites W2075747016 @default.
• W659235061 cites W2078177001 @default.
• W659235061 cites W2078271220 @default.
• W659235061 cites W2078711059 @default.
• W659235061 cites W2079854701 @default.
• W659235061 cites W2081215513 @default.
• W659235061 cites W2081696323 @default.
• W659235061 cites W2084720421 @default.
• W659235061 cites W2089045238 @default.
• W659235061 cites W2089462565 @default.

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